Geography Reference
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canonical measures are exclusively used to generate in following sections equidistant, conformal,
and equiareal mappings of various surfaces like the ellipsoid-of-revolution to the sphere. Hilbert's
invariant theory is finally used to generate scalar functions of the tensor-valued deformation
measures. Box 1.47 reviews the two fundamental Hilbert invariants of the Cauchy-Green arid
Euler-Lagrange deformation tensors.
2
l
2
Box 1.46 (Canonical criteria for a conformal, equiareal, and isometric mapping
M
M
r as
well as for an equidistant mapping c l ( t )
c r ( t )).
Conformeomorphism:
Λ 1 = Λ 2 or λ 1 = λ 2 ,
(1.300)
K 1 = K 2 or κ 1 = κ 2 ,
for all points of
r , respectively .
Areomorphism :
Λ 1 Λ 2 =1 or λ 1 λ 2 =1 ,
l or
M
M
(1.301)
K 1 K 2 + 1
2 ( K 1 + K 2 )=0 or κ 1 κ 2 + 1
2 ( κ 1 + κ 2 )=0 ,
2
2
for all points of
r , respectively .
Isometry :
Λ 1 = Λ 2 =1 or λ 1 = λ 2 =1 ,
M
l or
M
(1.302)
K 1 = K 2 =0 or κ 1 = κ 2 =0 ,
for all points of
1 , respectively .
Equidistance:
Λ 1 =1 , Λ 2 =1or λ 1 =1 , λ 2 =1 .
l or
M
M
(1.303)
K 1 =0 , K 2 =0or κ 1 =0 , 2 =0 .
for all points of M
l (left curve) and M
r (right curve) which are equidistantly mapped.
Box 1.47 (Canonical representation of Hilbert invariants derived from deformation measures).
I 1 (C l ):= Λ 1 + Λ 2 =tr[C l G l ]
s i 1 (C r ):= λ 1 + λ 2 =tr[C r G r ] ,
(1.304)
I 2 (C l ):= Λ 1 Λ 2 =det[C l G l ]
i 2 (C r ):= λ 1 λ 2 =det[C r G r ] ,
ers s
or
I 1 (E l ):= K 1 + K 2 = tr[E l G l ]
s i 1 (E r ):= κ 1 + κ 2 = tr[E r G r ] ,
(1.305)
i 2 (E r ):= κ 1 κ 2 =det[E r G r ] .
I 2 (E l ):= K 1 K 2 =det[E l G l 1]
versus
 
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